So what does this statement intend to communicate? I don't think anyone here is suggesting that a ball will instantaneously right-angle move (notch-move). I believe, just like everyone else here does, that a ball moving through air that is not hit by a bat (for example) will have a smooth path. I do not believe this is an issue in debate. The issue in debate is "late break" and its existence potentially due to Reynolds and its relationship to Magnus.
From this especially you should know that this is a statistically insignificant sample. Unless the laws of statistics has changed since my post-graduate education a sample size needs to at least be 30 or greater. Then in my pragmatic experience in life, and relating this again to the riseball in softball pitchers, I have and very well could catch 12 different pitchers and never see a pitcher with "late-break".
Let's break this down in a comparative analysis between what you are saying and what MIT folks have said. You are saying Reyonolds can not have an effect over a baseball pitched across over 60 feet. But the MIT folks say that Reynolds is in play over a 66 foot cricket pitch. Are you suggesting that this less than six feet delta is the critical difference? But before you answer that you might want to remember that a cricket ball is heavier and much smoother than a baseball which then those facts really place your contention in doubt.
I want to suggest again here, that you, then we, are getting very confused on your consistent use of the word "smooth". AGAIN a "smooth" path is NOT the question in debate,..... LATE BREAK is.
I don't have time right now to answer all your questions in detail. You are certainly correct that I use the word "smooth" without really defining what I mean by that, since I am trying to avoid technical language. Virtually every pitched ball trajectory I have analyzed can be described by constant acceleration in each of the three dimensions. That type of model can be improved upon slightly by allowing the accelerations to be dependent on the square of the velocity. That is what I mean by smooth. Regarding "late break", I have no opinion about that, since that term has different meaning for different people. The trajectories that people have been posting here (taken from data I have provided, by the way) all are smooth according to the definition I gave you. Whether some of you think they show late break or not is not important to me. They are what they are, regardless of what you call them.
I have not seen the MIT data. If you can provide a link to it, I will take a look. However, you made the important observation that a cricket ball is smoother than a baseball. That actually makes a big difference in the drag crisis, which is a very sharp transition for a smooth ball but not for a baseball, the latter based on real measurements. I am not sure I have seen data for a softball, but I would guess it would look more like a baseball than a smooth ball. So, while I agree that the effect you are talking about can occur in principle, I am very doubtful that it can occur for a pitched baseball or softball. And in any case, such an effect is not consistent with lots of data.
I don't understand your argument about statistics and sample size. As I have said, I have looked at many thousands of MLB pitches from many different pitchers. Are you in effect saying that the "late break" is so infrequent that one needs to look at huge numbers of pitches to find one?